the strong wind shear , a large , deep burst of convection formed in the northern semi ##ci ##rcle of josephine . the center was found to have shifted towards the new convection leading to an increase in intensity . the forecast showed a slight decrease in wind shear as josephine continued westward and no change in intensity over the 5 @ - @ day forecast was predicted . however , the convection decreased once more and the low became completely exposed by the late morning hours and josephine weakened again . by the afternoon , the center of josephine was only a swirl of clouds , devoid of convection . during the overnight hours on september 4 into the morning of september 5 , convection associated with
the strong wind shear, a large, deep burst of convection formed in the northern semicircle of josephine. the center was found to have shifted towards the new convection leading to an increase in intensity. the forecast showed a slight decrease in wind shear as josephine continued westward and no change in intensity over the 5 @ - @ day forecast was predicted. however, the convection decreased once more and the low became completely exposed by the late morning hours and josephine weakened again. by the afternoon, the center of josephine was only a swirl of clouds, devoid of convection. during the overnight hours on september 4 into the morning of september 5, convection associated with